From Fe Li rich micas to lepidolite and muscovite: The magmatic to hydrothermal evolution of phyllosilicates in the apical zone of the Beauvoir granite (French Massif Central)
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From Fe Li rich micas to lepidolite and muscovite: The magmatic to hydrothermal evolution of phyllosilicates in the apical zone of the Beauvoir granite (French Massif Central) | Researchclopedia